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Closed-Form Models for Nonisothermal Effective Stress of Unsaturated Soils

机译:非饱和土的非等热有效应力的闭合模型

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摘要

Effective stress is a critical factor controlling the mechanical behavior of unsaturated soils. There has been an increasing interest toward fundamental and applied research on emerging applications that involve unsaturated soils subjected to elevated temperatures. However, major gaps remain in the development of a unified model that can properly represent temperature dependency of effective stress in unsaturated soils. The main objective of this study is to develop closed-form equations to describe the effective stress of unsaturated soils under nonisothermal conditions. For this purpose, suction stress-based formulations are developed for representing temperature-dependent suction stress and effective stress of unsaturated soils. The formulations incorporate temperature-dependent moist air pressure and matric suction into a skeleton stress equation originally developed using volume averaging. A nonisothermal soil water retention curve (SWRC) is used to account for thermal effects on the adsorbed water, surface tension, contact angle, and enthalpy of immersion per unit area. The validity of the model is examined by comparing predicted suction stress values against experimental data reported in the literature for various soils ranging from clay to sand. The effective stress equations developed in this study can provide further insight into the behavior of unsaturated soils under nonisothermal conditions. The models can be readily incorporated in numerical and analytical methods, leading to more accurate modeling of unsaturated soils subjected to nonisothermal loading conditions.
机译:有效应力是控制不饱和土的力学行为的关键因素。对新出现的应用的基本和应用研究越来越兴趣,这些应用涉及不饱和土壤经受升高的温度。然而,主要间隙仍然是在统一模型的发展中,可以正确地代表不饱和土壤的有效应力的温度依赖性。本研究的主要目的是开发闭合形式方程,以描述非热条件下不饱和土壤的有效应力。为此目的,开发了用于代表温度依赖性的抽吸应力和不饱和土壤的有效应力的制备基于胁迫的配方。制剂掺入温度依赖性湿气压力和最初使用体积平均开发的骨架应力方程中的湿气抽吸。非等温土壤水保留曲线(SWRC)用于考虑每单位区域的吸附水,表面张力,接触角和浸泡焓的热效应。通过比较从文献中报告的各种土壤的实验数据的预测抽吸应力值进行了对粘土的各种土壤的实验数据来检查模型的有效性。本研究中开发的有效应力方程可以进一步了解非温条件下不饱和土的行为。该模型可以容易地以数值和分析方法掺入,导致更准确地建模不饱和土壤受到非等温载荷条件。

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